来自马丹矿区的米勒铁矿

Review of the Bulgarian Geological Society Pub Date : 2023-12-01 DOI:10.52215/rev.bgs.2023.84.3.67

P. Petrov

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引用次数: 0

摘要

在马丹矿区的克鲁舍夫多尔（Krushev Dol）和莫吉拉塔（Mogilata）矿床的样本中发现了米勒铁矿。在两种不同外观和矿物成分的集合体中发现了它。其中一种与浅绿色的铁罗托洛莫来石伴生，另一种与翠绿色的水帘石（含铬辉石）伴生。在一些分析中只检测到钴和铁作为杂质元素。它们的浓度很小（低于 0.01 apfu）。镍/硫比率为 0.95。镍源与被含矿脉切割的蛇纹石化超闪长岩体有关。

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Millerite from the Madan ore field

Millerite is discovered in samples from Krushev Dol and Mogilata deposits in the Madan ore field. It was found in two associations different in appearance and mineral composition. One of them is with light green ferrodolomite, and the other with bright green mariposite (chromium-bearing phengite). Only cobalt and iron are detected as impurity elements in some analyses. They are in small concentrations (below 0.01 apfu). The Ni/S ratio is 0.95. The nickel source is associated with bodies of serpentinized ultramafics cut by ore-bearing veins.

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Review of the Bulgarian Geological Society

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